Econ. Environ. Geol. 2013; 46(6): 581-592
Published online December 31, 2013
© THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY
Correspondence to : hsy@pusan.ac.kr
In this study, the chemical components (pH, HCO3-, Cl-, and SO42-) of water sources (surface water, groundwater, and spring water) in 1930s were compared to those in the period of 1985?1992 in Jeju Island. By the comparison, pH values and Cl-, and SO42- concentrations in 1930s appeared similar to those in the second period (1985?1992) while HCO3- increased about the six times in the second period. Such a great increase of HCO3- concentration may be caused by the increase of carbon dioxide in the atmosphere due to industrialization.
Keywords Jeju Island, 1930s, water source, water quality, carbon dioxide
Econ. Environ. Geol. 2013; 46(6): 581-592
Published online December 31, 2013
Copyright © THE KOREAN SOCIETY OF ECONOMIC AND ENVIRONMENTAL GEOLOGY.
Hong-Il Kwon1, Yun-Yeong Oh1, Yoon-Suk Park2, Kangjoo Kim3 and Se-Yeong Hamm1*
1Division of Earth Environmental System, Pusan National University, Busan 609-735, Korea
2Jeju Water Resources headquarters, Jeju Special Self-Governing Province 695-962, Korea
3Department of Environmental Engineering, Kunsan National University, Kunsan 573-701, Korea
Correspondence to:hsy@pusan.ac.kr
In this study, the chemical components (pH, HCO3-, Cl-, and SO42-) of water sources (surface water, groundwater, and spring water) in 1930s were compared to those in the period of 1985?1992 in Jeju Island. By the comparison, pH values and Cl-, and SO42- concentrations in 1930s appeared similar to those in the second period (1985?1992) while HCO3- increased about the six times in the second period. Such a great increase of HCO3- concentration may be caused by the increase of carbon dioxide in the atmosphere due to industrialization.
Keywords Jeju Island, 1930s, water source, water quality, carbon dioxide
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